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Updated: Aug 2, 2026

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Extraction and Characterization of Surfactants from Atmospheric Aerosols
Published on: April 21, 2017
極地層の平流層雲における窒素酸三水素 (NAT)
C Voigt1, J Schreiner, A Kohlmann
1Max-Planck-Institut für Kernphysik, Division of Atmospheric Physics, Post Office Box 103 980, D-69029 Heidelberg, Germany.
まとめ
極地層の平流層雲には,氷の形成温度より上にある窒素酸三水素 (NAT) 粒子が含まれています. これらのNAT粒子は,極地におけるオゾン層の減少に寄与する.
科学分野:
- 大気化学 大気化学
- 極地気象学 極地気象学
背景:
- 極地平流層雲 (PSC) は,極地オゾン層の減少に重要な役割を果たしています.
- PSCの組成を理解することは,大気モデリングに不可欠です.
研究 の 目的:
- PSCの構成を調査する.
- PSCにおける窒酸三水素 (NAT) 粒子の存在を確認する.
主な方法:
- スウェーデンのキルナから発射された気球搭載機器.
- 20~24kmの高さの雲層のインシトゥ測定.
主要な成果:
- PSCの層は,標高20~24kmの間に観測されました.
- 粒子の分析により,窒素酸三水素 (NAT) 粒子の有意な割合が明らかになりました.
- NAT粒子は,氷形成点以上の温度で存在していました.
結論:
- 固体NAT粒子は,氷形成よりも高い温度でPSCに存在します.
- NAT粒子の存在は,塩素の活性化を促進し,オゾン破壊につながります.
- この発見は,極地冬の初期と後半のオゾン層の減少に特に関連しています.
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